Synchrotron X-ray powder diffraction experiments have been performed on dehydrated Csexchanged natrolite to systematically investigate successive transitions under high pressures and temperatures. At pressures above 0.5(1) GPa using H 2 O as a pressure-transmitting medium and after heating to 100 °C, dehydrated Cs 16 Al 16 Si 24 O 80 (deh-Cs-NAT) transforms to a hydrated phase Cs 16 Al 16 Si 24 O 80 ·16H 2 O (Cs-NAT-II), which has a ca. 13.9% larger unit-cell volume. Further compression and heating to 1.5 GPa and 145 °C results in the transformation of Cs-NAT-II to Cs 16 Al 16 Si 32 O 96 (anh-Cs-POL), a H 2 O-free pollucite-like triclinic phase with a 15.6% smaller unit-cell volume per 80 framework oxygen atoms (80O f ). At pressures and temperatures of 3.7 GPa and 180 °C, a new phase Cs 1.547 Al 1.548 Si 6.452 O 16 (Cs-HEX) with a hexacelsian framework forms, which has a ca. 1.8% smaller unit-cell volume per 80O f . This phase can be recovered after pressure release. The structure of the recovered Cs-HEX has been refined in space group P6 3 /mcm with a = 5.3731(2) Å and c = 16.6834(8) Å, and also been confirmed by HAADF-STEM real space imaging. Similar to the hexacelsian feldspar (i.e., BaAl 2 Si 2 O 8 ), Cs-HEX contains Cs + cations that act as bridges between the upper and lower layers composed of tetrahedra and are hexa-coordinated to the upper and lower 6-membered ring windows. These pressure-and temperature-induced reactions from a zeolite to a feldspar-like material are important constraints for the design of materials for Cs + immobilization in nuclear waste disposal.